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Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
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Cretaceous ‘superchron’
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Pacific Antarctic ridge Schematic model
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Drummond Matthews (left) and Fred Vine Cambridge University
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Magnetic anomalies over the Reykjanes Ridge (S. of Iceland) from Vine & Matthews (1963). Positive anomalies are colored, negative ones are white.
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Magnetic anomaly patterns acquired by the oceanic crust, while it formed during the Gilbert Reversed Chron (top) and afterwards (from Vine & Matthews, 1963) Gauss Matuyama Brunhes (today) Gilbert
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Juan de FucaEast Pacific Rise observed mirror image model
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Relative spreading rates
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Blanco fracture zone
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Alfred Wegener
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Wegener’s map (1910). Note the distortion of India. Map made with a computer (1965).
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The meaning of an “apparent” polar wander path (APWP).
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S. Keith Runcorn (1922 – 1995)
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Computer-generated fit of the Atlantic- bordering continents (Bullard et al., 1965), minimizing gaps and overlaps.
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Ages of the Ocean floor determined from magnetic anomalies (~ 1990)
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Late Cretaceous (~85 Ma) map of the world (Scotese, 1981) www.scotese.com
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Magnetic field during reversals
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Geodynamo simulations (Glatzmaier and Roberts, 1996) Inner core Outer core High fluid velocity in tangent cylinder
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Magnetic field lines Close up of inner core
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